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Different vegetation patterns have difference influenced on the soil nutrients and the soil nutrient contents of different soil layers in the same vegetation patterns are also different in size. In this paper, we analyze the main soil nutrients of different soil layers in different vegetation patterns in Huanghuadianzi small watershed in Ao HanQI of Chifeng in China. The result shows that in different vegetation patterns, the secondary forest of natural bush have an obvious effect on the nutrient and concentration of organic; in the artificial forest, mingled forest has a better improving effect on soil than the pure forest and natural grassland has the smallest effect; in the same vegetation patterns, organic, total nitrogen present an overall reduction trend with the deepening of soil layer accept 40-60cm soil layers. The analysis result of this paper can provide a theoretical basis for further researching the dynamic nutrient change, tree variety optimization arrangement and regional land use planning in forest grass zone.

From a greenhouse gas policy standpoint, forests play an extremely important role in the exchange of carbon dioxide between the land and atmosphere. Because forest management has a potentially large effect on the entire forest carbon (C) cycle, and the biological and industrial systems are tightly coupled in the North region of China, simulation of varying management and forest product production scenarios are needed to explore trade-offs of managing forests for multiple objectives. Thus, an important consideration in management of forests is their present and future capacity to sequester C from the atmosphere. In this paper, C balance of the biological system was simulated under different management scenarios that were designed to test effects of plant configuration.

This research was conducted in Huanghuadianzi watershed in Aohan, Chifeng, Inner Mongolia. Geostatistic was used to study the spatial distribution of soil nitrogen and their affecting factors. The results showed that the soil nitrogen contents in all layers distributed as an island shape, and the high value areas were mainly distributed in the northwest of the watershed as an obvious fertile island shape, while the low value areas were mainly distributed in the south of the watershed. Nitrogen was mainly concentrated in the surface soil, and its content decreased with the increase of soil depth. The soil nitrogen content at first increased then decreased with the altitude, decreased with the slope, and showed the order of shady slopesemi-shady slopesemi-sunny slopesunny slope in different aspects. The average soil nitrogen contents in different land use types ranked as croplandwoodlandgrassland.